Radiation Processes - Sinica
Transcript of Radiation Processes - Sinica
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Radiation Processes
Hiroyuki Hirashita (平下 博之) Room 1320
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1. Electromagnetic Radiation
All wavelengths are important in astronomy!
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Radiation Mechanisms
Bremsstrahlung (free–free)
e-
p+
Ionized gas: e.g., H II region Intracluster medium
Synchrotron (magnetic bremsstrahlung)
B
e-
Supernovae AGN jet
Radiation ⇔ Acceleration of electric charge
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Radiation as Photonselectric ~ UV, optical molecular vibrational ~ near-IR molecular rotational ~ radio
Radiative transition
(Inverse) Compton Radiation
e- hν hνIntracluster medium (Sunyaev-Zeldovich effect) AGN jet, accretion disk
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F⌫ =
II⌫ cos � d�
2. Radiation Transfer EquationDefinition of Intensity (energy flow on a line) dE = Iν dA dt dΩ dν Iν [erg/cm2/s/sr/Hz]
dA
dΩ
Definition of Flux (net energy flow through a surface) Fν [erg/cm2/s/Hz]
dA
dΩ
Iν
θn
n
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dI⌫ds
= �⌫⇢I⌫ + j⌫
What is Radiation Transfer Equation?
s
absorbing and emitting medium
Iν(s): intensity
Emission jν [erg/cm3/s/Hz]Absorption
κν [cm2/g]: mass absorption coefficient ρ [g/cm3]: density
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Absorption
Total absorbing area: σν(n dA ds) n: number density of the absorber σν: absorption cross section of the absorber ⇒ −dIν dA = Iν(nσνdA ds) ⇒ dIν = −nσνIν ds
nσν = ρκν ρ: mass density (= mn; m is the mass of the absorber) κν: mass absorption coefficient
ds
dA
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Optical Depth
Optical depth: dτν = ρκνds (= nσνds) dIν /dτν= −Iν + Sν
Sν = jν/(ρκν): source function
τν
absorbing and emitting medium
Iν(τν): intensity
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3. Thermal Equilibrium
T
dIν/dτν = −Iν + Sν Iν = Bν is satisfied only if Sν = Bν: Local thermodynamic equilibrium (LTE).
T
Bν(T)
Iν
Thermal Radiation: Sν = Bν
(jν = ρκνBν): Kirchhoff’s law
Intensity = Planck function:
Blackbody radiation
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The Properties of Bν(T)(1) Monotonic increase
with T. (2) Peak (∂Bλ/∂λ|λ = λmax =
0): λmaxT = 0.29 cm deg (Wien displacement law).
(3) hν << kT ⇒ Bν(T) ~ (2ν2/c2)kT (Rayleigh-Jeans law)
(4)
€
πBν (T)dν =σT 40
∞
∫σ = 2π5k4/(15c2h3) Stefan-Boltzmann constant
€
Bν (T) =2hν 3 /c 2
exp(hν /kT) −1
Bλ(T) =2hc 2 /λ5
exp(hc /kλT) −1
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4. Some Simple Solutions of the RT Equation
For thermal radiation with a constant T,
I⌫(⌧⌫) = I⌫(0)e�⌧⌫ +B⌫(1� e�⌧⌫ )
τν
absorbing and emitting medium
Iν(τν): intensityIν(0)
dIν /dτν= −Iν + Sν ⇒
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I⌫(⌧⌫) = I⌫(0)e�⌧⌫
Ex. 1: Absorption of Background LightIf Iν >> Bν (T) (cold medium in front of a bright source)
Application 1: Absorption lines (measurement of the abundance)
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Dark clouds in the Milky Way ← Dust extinction (= absorption + scattering)
Ex. 1: Absorption of Background LightApplication 2: Dust extinction in the Milky Way
Optical (λ ~ 0.5 µm) Lund Observatory
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I⌫(⌧⌫) = B⌫(1� e�⌧⌫ )
Ex. 2: Emission and Self-Absorption
No background source:
Optically thin: τν << 1 ⇒ Iν = Bντν = κνρLBν
Optically thick: τν >> 1 ⇒ Iν = Bν
Directly reflects the temperature, but the information on internal details is not obtained (or we can only see the surface).
τνIν(τν): intensity
L
column density
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Example of Optically Thick Radiation
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Applications of Optically Thin Case
(1) Estimate of column density (ρL) if optical properties are known.
(2) Estimate of optical properties (κν): especially the wavelength dependence.
Optically thin: τν << 1 ⇒ Iν = Bντν = κνρLBν
I⌫(⌧⌫) = B⌫(1� e�⌧⌫ )
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Estimate of Column Density: Atomic Hydrogen (21 cm)
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Optical Properties of Dust
Li & Draine (2001)
Large grains (LGs) Silicate + carbonaceous material
Excess by very small grains (VSGs)
Wavelength (µm)
Inte
nsity
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5. The Einstein Coefficientslevel 2 Spontaneous emission
A21 (transition probability per unit time)
hν
level 1level 2
hν
level 1
Absorption B12J (transition probability per unit time)
level 2
level 1
Stimulated emission B21J (transition probability per unit time)
hν
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J = Jνφ(ν)dν0
∞
∫
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φ(ν)dν =10
∞
∫φ(ν): line profile function
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Einstein Relations
should be the Planck function.
Thermodynamic equilibrium n1B12J = n2A21 + n2B21J ⇒
g1B12 = g2B21 A21 = (2hν3/c2)B21
€
J =A21 /B21
(n1 /n2)(B12 /B21) −1
€
n1n2
=g1g2exp(hν /kT)
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J =A21 /B21
(g1B12 /g2B21)exp(hν /kT) −1
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Absorption and Emission Coefficients
Using the Einstein relations,€
jν =hν4π
n2A21φ(ν)
€
αν =hν4π
φ(ν )(n1B12 − n2B21)
€
Sν =n2A21
n1B12 − n2B21
€
αν =hν4π
n1B12(1− g1n2 /g2n1)φ(ν )
€
Sν =2hν 3
c 2g2n1g1n2
−1⎛
⎝ ⎜
⎞
⎠ ⎟
−1
The above equation holds also for nonthermal emission Derive αν and Sν for LTE!
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Further Reading
• Rybicki, G. B., & Lightman, A. P. 1979, “Radiative Processes in Astrophysics”, (Wiley: New York)